JEQ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in J Environ Qual 10:482-486 (1981)
© 1981 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Dendy, F. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Dendy, F. E.
Agricola
Right arrow Articles by Dendy, F. E.

Sediment Yield from a Mississippi Delta Cotton Field1

F. E. Dendy2

ABSTRACT

Sediment yield from flat (0.2% slope) delta fields was measured during a 33-month study. Annual erosion rates were higher than anticipated, ranging from a maximum 12 metric tons ha–1 for a year of above normal rainfall to a minimum 5 metric tons ha–1 for a year of slightly below normal rainfall. Highest sediment concentrations in runoff occurred in the spring during the seedbed preparation and planting season when the soil was bare of vegetative cover, freshly plowed, and highly susceptible to erosion. Lowest concentrations occurred in September and October when vegetative cover was good.

Sediment particle size data from selected storms showed that about 83% of the sediment removed from the fields was < 2 µm in diameter and nearly all, 98% was < 16 µm. Field soils were composed of 24% clay, 23% silt, and 53% sand, so considerable enrichment of fine particles occurred during the erosion process. This indicates that most sediment deposits in streams and lakes of the area are composed of fine materials and that gradual enrichment of coarse particles in the soils is occurring over long periods of time.

Key Words: sediment particle size • sediment concentration • runoff • erosion control


NOTES

1 Contribution of the USDA Sedimentation Laboratory, Delta States Area, USDA-SEA-SR, Oxford, MS 38655.

2 Research Hydraulic Engineer, USDA Sedimentation Lab., Oxford, Miss.

Received for publication February 14, 1981.


This article has been cited by other articles:


Home page
Journal of Soil and Water ConservationHome page
M.A. Locke, S.S. Knight, S. Smith Jr., R.F. Cullum, R.M. Zablotowicz, Y. Yuan, and R.L. Bingner
Environmental quality research in the Beasley Lake watershed, 1995 to 2007: Succession from conventional to conservation practices
Journal of Soil and Water Conservation, November 1, 2008; 63(6): 430 - 442.
[Abstract] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 1981 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.